
metamorphic
Iron-stained quartz-rich rock, possibly jasper or altered quartzite
Uncertain; likely microcrystalline quartz (SiO₂) with iron oxides/hydroxides
AI-generated identification · may be incorrectHardness about 6.5–7; ochre-yellow to brown with gray, glassy-to-waxy areas and irregular massive texture. Likely no visible cleavage, conchoidal-to-uneven fracture, and moderate-to-high specific gravity from iron staining; the image is insufficient for a definitive identification.
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Physical properties
Hardness about 6.5–7; ochre-yellow to brown with gray, glassy-to-waxy areas and irregular massive texture. Likely no visible cleavage, conchoidal-to-uneven fracture, and moderate-to-high specific gravity from iron staining; the image is insufficient for a definitive identification.
Formation & geological history
Silica-rich material may have formed as chert/jasper or quartzite, later fractured and stained by groundwater carrying hematite and limonite. Exact age and formation environment cannot be determined visually.
Uses & applications
Potentially suitable as a lapidary or display specimen if it takes a polish; iron-rich jasper is also used for cabochons, beads, and decorative stone. It has little construction value as an individual piece.
Geological facts
Yellow-brown coloration commonly reflects limonite/goethite coatings or replacement, while gray translucent zones may be quartz. A streak, hardness, acid, and specific-gravity test would substantially improve identification.
Field identification & locations
Commonly found in weathered quartz veins, chert beds, iron-rich soils, and metamorphic terrains worldwide. Test whether it scratches glass, leaves a yellow-brown streak, and reacts to dilute hydrochloric acid; avoid assuming it is gold-bearing from its color.
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